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Experimental soil studies to estimate the nitrate load of the groundwater in the water protection areas of the island Fohr

机译:土壤实验研究,以评估福尔岛水域保护区内地下水的硝酸盐负荷

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At the Island Fohr water protection areas were established in 1985 because of the rising values of nitrate in the groundwater of the waterworks since the beginning of the eighties. Even a voluntary limitation of the intensity of agricultural landuse and an increasing afforestation of low productivity regions since 1975 did not show any effect on the groundwater until 1990. The siols in the water protection areas were soil-mapped, and to evaluate the release of nitrate from the surface soil with the new formed groundwater an in situ-incubation experiment to evaluate the mineralisation of nitrogen was set over one year at five locations. Out of this results combined with a climatic water balance nitrate concentrations in the new formed groundwater were calculated which are similar to those of the groundwater of the waterworks. It is concluded that in the past 30 years the widespread "Plaggenboden" were overload with nitrogen. That means that the C/N relation was forced more tightly, and the nitrogen content of the upper soil was nearly doubled. That induces an increasing biological activity with rising rates of nitrogen mineralisation.
机译:由于80年代初以来自来水厂地下水中硝酸盐的含量不断上升,因此在Island Fohr建立了水保护区。自1975年以来,即使是自愿限制农业用地强度和增加低生产率地区的绿化,直到1990年都没有对地下水产生任何影响。水保护区中的硅醇被土壤覆盖,并评估硝酸盐的释放从地表土壤中注入新形成的地下水,在五个地点进行了一年的原位温育实验,以评估氮的矿化作用。从这些结果中,结合气候水平衡,计算出新形成的地下水中的硝酸盐浓度与自来水厂的地下水浓度相似。结论是,在过去的30年中,普遍存在的“ Plaggenboden”富含氮。这意味着C / N关系被迫更紧,上层土壤的氮含量几乎翻了一番。随着氮矿化速率的增加,生物活性随之增加。

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